Geomorphological settings for past increases of the levels of great Mongolian and Mongolia-Russia transboundary lakes

Standard

Geomorphological settings for past increases of the levels of great Mongolian and Mongolia-Russia transboundary lakes. / Krtvonogov, Sergey; Narantsetseg, Tserendash; Oyunchimeg, Tserentsegmid et al.

In: Chikei/Transactions, Japanese Geomorphological Union, Vol. 41, No. 3, 08.2020, p. 227-248.

Research output: Contribution to journal › Article › peer-review

Harvard

Krtvonogov, S, Narantsetseg, T, Oyunchimeg, T, Agatova, A, Khazin, L, Nepop, R, Zhilich, S, Kuleshov, D & Gusev, V 2020, 'Geomorphological settings for past increases of the levels of great Mongolian and Mongolia-Russia transboundary lakes', Chikei/Transactions, Japanese Geomorphological Union, vol. 41, no. 3, pp. 227-248.

APA

Krtvonogov, S., Narantsetseg, T., Oyunchimeg, T., Agatova, A., Khazin, L., Nepop, R., Zhilich, S., Kuleshov, D., & Gusev, V. (2020). Geomorphological settings for past increases of the levels of great Mongolian and Mongolia-Russia transboundary lakes. Chikei/Transactions, Japanese Geomorphological Union, 41(3), 227-248.

Vancouver

Krtvonogov S, Narantsetseg T, Oyunchimeg T, Agatova A, Khazin L, Nepop R et al. Geomorphological settings for past increases of the levels of great Mongolian and Mongolia-Russia transboundary lakes. Chikei/Transactions, Japanese Geomorphological Union. 2020 Aug;41(3):227-248.

Author

Krtvonogov, Sergey ; Narantsetseg, Tserendash ; Oyunchimeg, Tserentsegmid et al. / Geomorphological settings for past increases of the levels of great Mongolian and Mongolia-Russia transboundary lakes. In: Chikei/Transactions, Japanese Geomorphological Union. 2020 ; Vol. 41, No. 3. pp. 227-248.

BibTeX

@article{45a4f4e95a8a4f518554e77bca813a70,

title = "Geomorphological settings for past increases of the levels of great Mongolian and Mongolia-Russia transboundary lakes",

abstract = "The paper discusses geomorphological aspects of former appearances of huge lakes in the Valley of Great Lakes, the Valley of Gobi Lakes in northwestern and western Mongolia and in depressions of northeastern Mongolia, and partly in bounding Russia. The problem is far from its solution, despite a progress with dating of the lake sediments reflected in recent publications. In the paper, we analyze morphometry of high levels of the lakes visible on the satellite images as series of shorelines, which are very young, not older than the Holocene age. The investigated lakes are terminal basins collecting waters from the catchments of large rivers draining the Altai, Khangai, and Khentey Mountains; two of them form more complicated lake systems: of the Khyargas Lake including several transitional lakes, and of the Torei - Khukh lakes. The discussing reasons for these rises are obviously climatic with possible high influences of the deglaciation processes in the surrounding mountains.",

keywords = "Central Asia, Geomorphology, Lake level changes, Mongolia, Paleolakes, Remote sensing, Russia, Terminal basins",

author = "Sergey Krtvonogov and Tserendash Narantsetseg and Tserentsegmid Oyunchimeg and Anna Agatova and Leonid Khazin and Roman Nepop and Snezhana Zhilich and Dmitry Kuleshov and Victor Gusev",

year = "2020",

month = aug,

language = "English",

volume = "41",

pages = "227--248",

journal = "Chikei/Transactions, Japanese Geomorphological Union",

issn = "0389-1755",

publisher = "Nippon Chikeigaku Rengo",

number = "3",

}

RIS

TY - JOUR

T1 - Geomorphological settings for past increases of the levels of great Mongolian and Mongolia-Russia transboundary lakes

AU - Krtvonogov, Sergey

AU - Narantsetseg, Tserendash

AU - Oyunchimeg, Tserentsegmid

AU - Agatova, Anna

AU - Khazin, Leonid

AU - Nepop, Roman

AU - Zhilich, Snezhana

AU - Kuleshov, Dmitry

AU - Gusev, Victor

PY - 2020/8

Y1 - 2020/8

N2 - The paper discusses geomorphological aspects of former appearances of huge lakes in the Valley of Great Lakes, the Valley of Gobi Lakes in northwestern and western Mongolia and in depressions of northeastern Mongolia, and partly in bounding Russia. The problem is far from its solution, despite a progress with dating of the lake sediments reflected in recent publications. In the paper, we analyze morphometry of high levels of the lakes visible on the satellite images as series of shorelines, which are very young, not older than the Holocene age. The investigated lakes are terminal basins collecting waters from the catchments of large rivers draining the Altai, Khangai, and Khentey Mountains; two of them form more complicated lake systems: of the Khyargas Lake including several transitional lakes, and of the Torei - Khukh lakes. The discussing reasons for these rises are obviously climatic with possible high influences of the deglaciation processes in the surrounding mountains.

AB - The paper discusses geomorphological aspects of former appearances of huge lakes in the Valley of Great Lakes, the Valley of Gobi Lakes in northwestern and western Mongolia and in depressions of northeastern Mongolia, and partly in bounding Russia. The problem is far from its solution, despite a progress with dating of the lake sediments reflected in recent publications. In the paper, we analyze morphometry of high levels of the lakes visible on the satellite images as series of shorelines, which are very young, not older than the Holocene age. The investigated lakes are terminal basins collecting waters from the catchments of large rivers draining the Altai, Khangai, and Khentey Mountains; two of them form more complicated lake systems: of the Khyargas Lake including several transitional lakes, and of the Torei - Khukh lakes. The discussing reasons for these rises are obviously climatic with possible high influences of the deglaciation processes in the surrounding mountains.

KW - Central Asia

KW - Geomorphology

KW - Lake level changes

KW - Mongolia

KW - Paleolakes

KW - Remote sensing

KW - Russia

KW - Terminal basins

UR - http://www.scopus.com/inward/record.url?scp=85102939089&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:85102939089

VL - 41

SP - 227

EP - 248

JO - Chikei/Transactions, Japanese Geomorphological Union

JF - Chikei/Transactions, Japanese Geomorphological Union

SN - 0389-1755

IS - 3

ER -

ID: 35675979